我们的网站为什么显示成这样?

可能因为您的浏览器不支持样式,您可以更新您的浏览器到最新版本,以获取对此功能的支持,访问下面的网站,获取关于浏览器的信息:

|Table of Contents|

敦化三大硬阔、红松年轮-气候关系及生长季低温重建(PDF)

《南京林业大学学报(自然科学版)》[ISSN:1000-2006/CN:32-1161/S]

Issue:
2013年03期
Page:
29-34
Column:
研究论文
publishdate:
2013-05-20

Article Info:/Info

Title:
Climate-growth relationships of three hardwood species and Korean pine and minimum temperature reconstruction in growing season in Dunhua, China
Author(s):
LI Mu WANG Xiaochun*
Center for Ecological Research, Northeast Forestry University, Harbin 150040, China
Keywords:
Fraxinus mandshurica-Juglans mandshurica-Phellodendron amurense-Pinus koraiensis tree rings growing season minimum temperature reconstruction Dunhua city
Classification number :
S716; P467
DOI:
10.3969/j.issn.1000-2006.2013.03.006
Document Code:
-
Abstract:
Dunhua is located at the hinterland of the Changbai Mountains in northern hemisphere high latitudes. It is one of the most significant areas of global climate change and typical broadleaved Korean pine forests in China. Three hardwood species(Fraxinus mandshurica, Juglans mandshurica and Phellodendron amurense)and Pinus koraiensis are main tree species of natural forests in this region. These species are critical to explore responses of boreal forests to climate change in northeast China. Dendrochronological methods were used to establish four standard chronologies of three hardwood species and P. koraiensis. Then, correlation analyses were made between these four chronologies and local climatic factors. The results showed that three hardwood species and P. koraiensis had similar responses to climatic factors. They were significantly and positively correlated with temperature,but was weakly correlated with precipitation. The growth of P. koraiensis was positively correlated with monthly minimum temperature in whole year, but the F. mandshurica had a strongest positively correlation with the minimum temperatures of January to October. The growth of Ph. amurense had a secondary relationship with temperature, which significantly and positively correlated with the temperature of February to September. J. mandshurica had a weak correlation with minimum temperature and it just was significantly correlated with May, June and September temperatures. In summary, temperature was the main limited factor for radial growth of broadleaved P. koraiensis forests in this region, especially for minimum temperature in growing season(April to September). Therefore, minimum temperature in growing season since 1854 in Dunhua was reconstructed by using mean chronology of three hardwoods and P. koraiensis. The reconstruction equation(Y = 4.28lnX + 8.774)explained 62.4% of the variance in minimum temperature. Segmented test proved that this reconstruction equation was stable. Variations of cool and warm periods were identical by comparing with previous studies. Reconstructed temperature of the last 158 years in this region showed there were three warmer periods(1860-1873, 1938-1947 and 1991-2010)and three cooler periods(1888-1933, 1965-1971 and 1977-1980)and warming up in last 30 years. There a minimum temperature change cycle were 8.4, 6.9-6.3, 3.7, 2.5 and 2.2 a in Dunhua.

References

[1] 尚华明,魏文寿,袁玉江,等.树木年轮记录的新疆新源350 a来温度变化[J].干旱区资源与环境,2011,25(9):187-190. Shang H M, Wei W S, Yuan Y J, et al. Variations of temperature during last 350 years at Xinyuan recorded by tree-ring[J]. Journal of Arid Land Resources and Environment, 2011, 25(9): 187-190.
[2] 邵雪梅,吴祥定.利用树轮资料重建长白山区过去气候变化[J].第四纪研究,1997(1):76-83. Shao X M, Wu X D. Reconstruction of climate change on Changbai Mountain, Northeast China using tree-ring data[J]. Quaternary Sciences, 1997(1): 76-83.
[3] 唐劲松,钱君龙,尹卓思,等.用树轮碳同位素年序列重建大气二氧化碳浓度[J].南京林业大学学报,2000,24(3):45-48. Tang J S, Qian J L, Yin Z S, et al. Restructing CO2 concentration by the tree ring carbon isotopic ratios of west Tianmu Mountain[J]. Journal of Nanjing Forestry University, 2000, 24(3): 45-48.
[4] 陈宝君,钱君龙,濮培民,等.树轮α-纤维素δ13C角分布及其气候学意义[J].南京林业大学学报:自然科学版,2002,26(1):14-18. Chen B J, Qian J L, Pu P M, et al. δ13C circumferential variation in tree-rings α-cellulose and its climatic implications[J]. Journal of Nanjing Forestry University:Natural Sciences Edition, 2002,26(1): 14-18.
[5] Qian W H, Zhu Y F. Climate change in China from 1880 to 1998 and its impact on the environmental condition [J]. Climatic Change, 2001, 50(4):419-444.
[6] 王蔚蔚,张军辉,戴冠华,等.利用树木年轮宽度资料重建长白山地区过去240年秋季气温的变化[J].生态学杂志,2012,31(4):787-793. Wang W W, Zhang J H, Dai G H, et al. Variation of autumn temperature over the past 240 years in Changbai Mountains of Northeast China: A reconstruction with tree-ring records[J]. Chinese Journal of Ecology, 2012, 31(4): 787-793.
[7] Zhu H F, Fang X Q, Shao X M, et al. Tree ring-based February-April temperature reconstruction for Changbai Mountain in northeast China and its implication for east Asian winter monsoon [J]. Climate of the Past, 2009(5):661-666.
[8] Yu D P, Wang Q M, Wang Y, et al. Climatic effects on radial growth of major tree species on Changbai Mountain [J]. Annals of Forest Science, 2011, 68(5):921-933.
[9] 朱连友,秦树林,郭建.敦化林业局森林资源动态分析[J].林业勘察设计,2011(1):15-17. Zhu L Y, Qin S L, Guo J.Analysis of forest resource dynamics in Dunhua city[J]. Forest Investigation Design, 2011(1): 15-17.
[10] 王传志,彭永凯,刘世清.敦化林区森林土壤调查[J].吉林林业科技,2003,32(6):49-50. Wang C Z, Peng Y K, Liu S Q. Forest soil survey in Dunhua[J]. Forestry Science and Technology,2003, 32(6): 49-50.
[11] Stokes M A, Smiley T L. An Introduction to Tree-ring Dating [M]. Chicago:The University of Chicago Press. 1968.
[12] Holmes R L. Computer assisted quality control in tree-ring dating and measurement [J]. Tree-ring Bulletin, 1983, 43:69-75.
[13] Cook E R, Kairiukstis L A. Methods of Dendrochronology. Applications in Environmental Sciences [M]. Dordrecht:Kluwer Academic Publishers. 1990.
[14] Cook E R, Meko D M, Stahle D W, et al. Drought reconstruction for the continental United States [J]. Journal of Climate, 1999, 12:1145-1162.
[15] Wigley T M L, Briffa K R, Jones P D. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology [J]. Journal of Climate and Applied Meteorology, 1984(23):201-213.
[16] 吴刚,梁秀英,张旭东,等.长白山红松阔叶林主要树种高度生态位的研究[J].应用生态学报,1999,10(3):262-264. Wu G, Liang X Y, Zhang X D, et al. Height niche of some tree species in the Korean pinebroad leaved forest on Changbai Mountain[J].Chinese Journalof Applied Ecology, 1999, 10(3): 262-264.
[17] 罗光裕,魏春茹.黄菠萝、胡桃楸、水曲柳营养器官结构的比较研究[J].东北林业大学学报,1991,19(S1):296-304. Luo G Y,Wei C R.Study on the comparison of vegetative organs structures of amurcork-tree,Manchurian walnut and Manchurian ash[J].Journal of Northeast Forestry University, 1991, 19(S1): 296-304.
[18] 赵西平,郭明辉,朱熙岭.温度对树木生长与木材形成影响的研究进展[J].森林工程,2005,21(6):1-4. Zhao X P, Guo M H, Zhu X L. Advance in research on the effects of temperature on trees growth and wood formation[J]. Forest Engineering,2005, 21(6): 1-4.
[19] Fredeen A L, Sage R F. Temperature and humidity effects on branchlet gas-exchange in white spruce:an explanation for the increase in transpiration with blanchlet temperature [J]. Trees, 1999, 14(3):161-168.
[20] 孙一荣,朱教君,于立忠,等.不同光强下核桃楸、水曲柳和黄菠萝的光合生理特征[J].林业科学,2009,45(9):29-35. Sun Y R, Zhu J J, Yu L Z, et al. Photosynthetic characteristics of Juglans mandshurica,Fraxinus mandshurica and Phellodendron amurense under different light regimes[J].Scientia Silvae Sinicae, 2009, 45(9): 29-35.
[21] 孙慧珍,孙龙,王传宽,等.东北东部山区主要树种树干液流研究[J].林业科学,2005,41(3):36-42. Sun H Z, Sun L, Wang C K, et al. Sapflow of the major tree species in the eastern mountainous region in Northeast China[J]. Scientia Silvae Sinicae, 2005, 41(3): 36-42.
[22] 张寒松.长白山典型植被树木年轮资料与气候变化的关系[D].哈尔滨:东北林业大学,2007. Zhang H S. Relationship between tree-ring chronology of representative species in Changbai Mountains and climate change[D]. Harbin: Northeast Forestry University, 2007.
[23] Wilson R, Arrigo R D, Buckley B, et al. A matter of divergence:Tracking recent warming at hemispheric scales using tree ring data[J].Journal of Geophysical Research:Atmosphere, 2007, 112(D16):103.
[24] Pachauri R K, Reisinger A. Contribution of working groups Ⅰ,Ⅱ and Ⅲ to the fourth assessment report of the intergovernmental panel on climate change[C]// Core writing team. Climate Change 2007:Synthesis Report, IPCC. Geneva, Switzerland. Cambridge University Press, Cambridge, 2007.
[25] 葛全胜,郑景云,满志敏,等.过去2 000 a中国东部冬半年温度变化序列重建及初步分析[J].地学前缘,2002,9(1):169-181. Ge Q S, Zheng J Y, Man Z M, et al. Reconstruction and analysis on the series of winter-half-year temperature changes over the past 2000 years in eastern China[J]. Earth Science Frontiers, 2002, 9(1): 169-181.
[26] McPhaden M J, Zebiak S E, Glantz M H. ENSO as an integrating concept in earth science [J]. Science, 2006, 314:1740-1745.

Last Update: 2013-05-31